Electromagnetic Induction Measurements near Ny Alesund ...

Electromagnetic induction is a non-invasive mapping technique used in a variety of applications including geological mapping and civil engineering, agriculture and forestry, environmental monitoring, groundwater protection, mineral exploration and archaeology. Electromagnetic induction is mainly use...

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Bibliographic Details
Main Authors: Uta Koedel, Claudia Schuetze, Peter Dietrich
Format: Dataset
Language:English
Published: Zenodo 2023
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.8289452
https://zenodo.org/doi/10.5281/zenodo.8289452
id ftdatacite:10.5281/zenodo.8289452
record_format openpolar
spelling ftdatacite:10.5281/zenodo.8289452 2024-01-28T10:08:33+01:00 Electromagnetic Induction Measurements near Ny Alesund ... Uta Koedel Claudia Schuetze Peter Dietrich 2023 https://dx.doi.org/10.5281/zenodo.8289452 https://zenodo.org/doi/10.5281/zenodo.8289452 en eng Zenodo https://dx.doi.org/10.5281/zenodo.8289451 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Polar MOSES AWIPEV Ny Alesund/Svalbard Geophysics FOS Earth and related environmental sciences Electromagnetic Induction EMI Long term observatory Bayelva 2023_MOSES_PolarMOSES Dataset dataset 2023 ftdatacite https://doi.org/10.5281/zenodo.828945210.5281/zenodo.8289451 2024-01-04T22:10:18Z Electromagnetic induction is a non-invasive mapping technique used in a variety of applications including geological mapping and civil engineering, agriculture and forestry, environmental monitoring, groundwater protection, mineral exploration and archaeology. Electromagnetic induction is mainly used to measure the (apparent) electrical conductivity of the subsurface, which depends on various soil properties such as clay content, water content and salinity. The nature and strength of the relationships between electrical conductivity and soil properties are site-specific. The instrument used, the EM38-MK2, measures both the quadrature (conductivity) and the inphase (magnetic susceptibility) components at two different depths, all at the same time, without the need for ground contact. The aim of the measurements was to improve the understanding of thaw-driven landscape dynamics in permafrost regions and to assess the vulnerability of permafrost to thaw. The measurements were carried out in August 2023 in the ... Dataset permafrost Svalbard DataCite Metadata Store (German National Library of Science and Technology) Bayelva ENVELOPE(11.898,11.898,78.933,78.933) Moses ENVELOPE(-99.183,-99.183,-74.550,-74.550) Svalbard
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Polar MOSES
AWIPEV
Ny Alesund/Svalbard
Geophysics
FOS Earth and related environmental sciences
Electromagnetic Induction EMI
Long term observatory Bayelva
2023_MOSES_PolarMOSES
spellingShingle Polar MOSES
AWIPEV
Ny Alesund/Svalbard
Geophysics
FOS Earth and related environmental sciences
Electromagnetic Induction EMI
Long term observatory Bayelva
2023_MOSES_PolarMOSES
Uta Koedel
Claudia Schuetze
Peter Dietrich
Electromagnetic Induction Measurements near Ny Alesund ...
topic_facet Polar MOSES
AWIPEV
Ny Alesund/Svalbard
Geophysics
FOS Earth and related environmental sciences
Electromagnetic Induction EMI
Long term observatory Bayelva
2023_MOSES_PolarMOSES
description Electromagnetic induction is a non-invasive mapping technique used in a variety of applications including geological mapping and civil engineering, agriculture and forestry, environmental monitoring, groundwater protection, mineral exploration and archaeology. Electromagnetic induction is mainly used to measure the (apparent) electrical conductivity of the subsurface, which depends on various soil properties such as clay content, water content and salinity. The nature and strength of the relationships between electrical conductivity and soil properties are site-specific. The instrument used, the EM38-MK2, measures both the quadrature (conductivity) and the inphase (magnetic susceptibility) components at two different depths, all at the same time, without the need for ground contact. The aim of the measurements was to improve the understanding of thaw-driven landscape dynamics in permafrost regions and to assess the vulnerability of permafrost to thaw. The measurements were carried out in August 2023 in the ...
format Dataset
author Uta Koedel
Claudia Schuetze
Peter Dietrich
author_facet Uta Koedel
Claudia Schuetze
Peter Dietrich
author_sort Uta Koedel
title Electromagnetic Induction Measurements near Ny Alesund ...
title_short Electromagnetic Induction Measurements near Ny Alesund ...
title_full Electromagnetic Induction Measurements near Ny Alesund ...
title_fullStr Electromagnetic Induction Measurements near Ny Alesund ...
title_full_unstemmed Electromagnetic Induction Measurements near Ny Alesund ...
title_sort electromagnetic induction measurements near ny alesund ...
publisher Zenodo
publishDate 2023
url https://dx.doi.org/10.5281/zenodo.8289452
https://zenodo.org/doi/10.5281/zenodo.8289452
long_lat ENVELOPE(11.898,11.898,78.933,78.933)
ENVELOPE(-99.183,-99.183,-74.550,-74.550)
geographic Bayelva
Moses
Svalbard
geographic_facet Bayelva
Moses
Svalbard
genre permafrost
Svalbard
genre_facet permafrost
Svalbard
op_relation https://dx.doi.org/10.5281/zenodo.8289451
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.5281/zenodo.828945210.5281/zenodo.8289451
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